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Variability and Predictability in Long- Range Predictions Arun Kumar Climate Prediction Center College Park, Maryland, USA arun.kumar@noaa.gov ICTP-IITM ESM Workshop 18 July, 2016 1/33 Outline What is weather and climate variability?


  1. Variability and Predictability in Long- Range Predictions Arun Kumar Climate Prediction Center College Park, Maryland, USA arun.kumar@noaa.gov ICTP-IITM ESM Workshop 18 July, 2016 1/33

  2. Outline • What is weather and climate variability? • What is predictability? • How is predictability quantified? • Sources of predictability • Estimating predictability • Realizing predictability (or prediction skill) ICTP-IITM ESM Workshop 18 July, 2016 2/33

  3. Weather and Climate Variability • Temperature tomorrow is not the same as today • Monthly (seasonal) mean precipitation for June-July-August seasonal average over India is not the same in 2014 as in 2015 • Average precipitation over India for a 10-year average changes from one decade to another ICTP-IITM ESM Workshop 18 July, 2016 3/33

  4. 2014 2015 ICTP-IITM ESM Workshop 18 July, 2016 4/33

  5. Annual Mean All India Temperature Anomaly ICTP-IITM ESM Workshop 18 July, 2016 5/33

  6. Quantifying Variability ICTP-IITM ESM Workshop 18 July, 2016 6/33

  7. Variance of 200-mb DJF Seasonal Mean Height ICTP-IITM ESM Workshop 18 July, 2016 7/33

  8. Predictability • Predictability: From the knowledge of the current state of the ocean, our ability to anticipate its future evolution • Prediction for a particular time-scale, what fraction of variability can be anticipated? – Predictability varies between 0-100% of variability ICTP-IITM ESM Workshop 18 July, 2016 8/33

  9. Why all the variability is not predictable? ICTP-IITM ESM Workshop 18 July, 2016 9/33

  10. There is always a spread (uncertainty) in forecasts! • Non-linear dynamical systems sensitivity to specification of initial conditions • Deterministic chaos • Uncertainty could be better quantified, but can never be removed ICTP-IITM ESM Workshop 18 July, 2016 10/33

  11. Example of Seasonal Prediction ICTP-IITM ESM Workshop 18 July, 2016 11/33

  12. Example of Climate Projection ICTP-IITM ESM Workshop 18 July, 2016 12/33

  13. • The forecast spread (uncertainty) can be quantified using ensemble prediction approach where a collection of forecasts is initiated from small perturbations in the initial conditions • In a nutshell – The reason for a limit on predictability stems from limits on the accuracy of predictions on shorter time-scales – One cannot always predict the state of the atmosphere ∆t from now with 100% accuracy no matter how small ∆t is. ICTP-IITM ESM Workshop 18 July, 2016 13/33

  14. How is Predictability Quantified? • Spread in forecast outcomes from different initial conditions can be quantified as probability density function (PDF) • It is our ability to distinguish PDF of outcomes for the event to be predicted from the climatological PDF • Differences in the PDF can come from differences in various moments of the PDF – Mean – Spread – Skewness ICTP-IITM ESM Workshop 18 July, 2016 14/33

  15. How is Predictability Quantified? Climatological PDF PDF for a Season (Red) ICTP-IITM ESM Workshop 18 July, 2016 15/33

  16. High predictability ICTP-IITM ESM Workshop 18 July, 2016 16/33

  17. Low predictability ICTP-IITM ESM Workshop 18 July, 2016 17/33

  18. Why it is Important to Understand and Quantify Predictability? • Helps gauge limits of prediction skill and manage expectations • Helps pinpoint sources of predictability, e.g., SST  for atmospheric variability • How do climate models simulate processes, physics and interactions to better predict “sources” of predictability? • Provides one way to focus model improvements • Where to place limited resources (ensemble size, model resolution, analysis, perturbations,…) ICTP-IITM ESM Workshop 18 July, 2016 18/33

  19. Sources of Predictability ICTP-IITM ESM Workshop 18 July, 2016 19/33

  20. Sources of Predictability Weather – Atmospheric initial conditions • Seasonal – Boundary conditions (upper oceans, soil moisture, snow, sea- ice…) • Decadal – deeper oceans,… • Climate projections – CO 2 ,… • For different lead time, the relative contribution from sources of predictability • differs ICTP-IITM ESM Workshop 18 July, 2016 20/33

  21. Influence of Various Factors on the PDF … initial conditions … boundary conditions … external conditions ICTP-IITM ESM Workshop 18 July, 2016 21/33

  22. Seasonal-to-Interannual - ENSO Sea Surface Temperature Anomaly ICTP-IITM ESM Workshop 18 July, 2016 22/33

  23. Decadal - PDO Sea Surface Temperature Anomaly (shading) ICTP-IITM ESM Workshop 18 July, 2016 23/33

  24. Estimating Predictability ICTP-IITM ESM Workshop 18 July, 2016 24/33

  25. Methods for Estimating Predictability • Observational data Daily time-series – Predictor – Predictand relationships – Analogs – Daily time-series DJF Z700 Correlation with SST index • Simple; unbiased, but non-linearity is hard to incorporate ICTP-IITM ESM Workshop 18 July, 2016 25/33

  26. Methods for estimating predictability • Models – Ensemble of integrations • Spread among the ensemble members is the unpredictable component • Ensemble mean (the common part) is the predictable component ICTP-IITM ESM Workshop 18 July, 2016 26/33

  27. Model Simulations ICTP-IITM ESM Workshop 18 July, 2016 27/33

  28. Decomposing Total Variability ICTP-IITM ESM Workshop 18 July, 2016 28/33

  29. Ratio of Predictable and Unpredictable Component 200mb Z ICTP-IITM ESM Workshop 18 July, 2016 29/33

  30. Realizing Predictability Predictability  Prediction skill • Requires a real-time forecast system • To realize predictability that exists, forecast systems need to have certain • attributes  Design and framework of long-range prediction systems (Thursday) • ICTP-IITM ESM Workshop 18 July, 2016 30/33

  31. Realizing Predictability ICTP-IITM ESM Workshop 18 July, 2016 31/33

  32. Implication of Limited Predictability • Since future outcomes are not certain, forecasts have to be probabilistic • Decision making under probabilistic information context is hard ICTP-IITM ESM Workshop 18 July, 2016 32/33

  33. Summary • There is variability associated with all time-scales • All variability cannot be anticipated in advance – Predictability • There are physical reasons that allow us to anticipate variability – sources of predictability • Predictability can be estimated either from observational data or model simulations • Forecast systems allow to realize predictability as prediction skill ICTP-IITM ESM Workshop 18 July, 2016 33/33

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